@Article{PadilhaVitoPáduFuck:2016:DeMaSi,
author = "Padilha, Antonio Lopes and Vitorello, {\'{\I}}caro and
P{\'a}dua, Marcelo Banik de and Fuck, Reinhardt Adolfo",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {Instituto Nacional de
Pesquisas Espaciais (INPE)} and {Universidade de Bras{\'{\i}}lia
(UnB)}",
title = "Deep magnetotelluric signatures of the early Neoproterozoic
Cariris Velhos tectonic event within the Transversal sub-province
of the Borborema Province, NE Brazil",
journal = "Precambrian Research",
year = "2016",
volume = "275",
pages = "70--83",
month = "Apr.",
keywords = "Northeast Brazil, Borborema Province, Magnetotellurics, Subduction
zone, Neoproterozoic, Cariris Velhos Orogeny.",
abstract = "The Borborema structural province, in northeast Brazil, consists
of a complex set of crustal blocks of different ages, origin and
evolution, with final amalgamation during the late Neoproterozoic
Brasiliano Orogeny. In the central part of the province, its
Transversal sub-province is characterized by elongate NE-SW
terranes largely affected by the Brasiliano metamorphic
overprinting and by a suite of early Neoproterozoic metavolcanic
and metaplutonic rocks, reflecting a distinct tectonic event
(Cariris Velhos). Magnetotelluric (MT) data were collected at 64
stations along four profiles across this central region of the
province to assess its deep electrical resistivity structure.
Dimensionality analysis shows that the subsurface is electrically
dominated by 3D structure, and 3D inversions of the full impedance
tensor and vertical magnetic transfer function (tipper) were
carried out. Data fit is relatively good with an acceptable
distribution of the misfit between the sites and the dominant
features in the final model are north-dipping crustal conductors,
which can be tentatively correlated between the different MT
profiles and cross contrasting terranes at the surface of the
province. Considering the geometry and distribution of the
conductors, it is proposed that they might reflect remnants of a
north-directed subduction zone with enhanced conductivity
associated with graphitized biogenic material in metasedimentary
rocks originally deposited in a restricted oceanic environment and
subsequently metamorphosed and introduced into the deep crust by
the subduction of the oceanic lithosphere. Constrained by isolated
outcrops of early Neoproterozoic rocks with oceanic affinity, the
proposed subduction event may have taken place during the Cariris
Velhos Orogeny with the crustal remobilization by the Brasiliano
Orogeny being restricted to the brittle upper crust. This
interpretation gives support for an accretionary model to the
Neoproterozoic geodynamic evolution of the Borborema Province.",
doi = "10.1016/j.precamres.2015.12.012",
url = "http://dx.doi.org/10.1016/j.precamres.2015.12.012",
issn = "0301-9268",
language = "en",
targetfile = "Padilha_deep.pdf",
urlaccessdate = "27 abr. 2024"
}